关于库尔干地区Zverinogolovskoye地区1-k岩心井钻探结果的问题

D. Leontiev, A. A. Arsenyev
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摘要

本文介绍了库尔干地区Zverinogolovskoye地区1 k岩心井的钻探结果和岩心材料的研究。一些研究人员对阿拉布加河上周期性出现油膜的原因是石油从深处迁移的事实表示怀疑。一些人认为它可能是偶然进入河流的,比如农民在田野工作时泄漏的。1959年,为了检查和研究阿拉布加河沿岸的石油情况,钻了1-k和2-k井。1-k井和2-k井穿过中新生代盖层,暴露出以红色花为代表的基底岩,推测为二叠纪-三叠纪。这使得研究沉积物的岩性和地层学成为可能,这些沉积物与该地区的构造有关。用1-k井芯测得的红色岩石的倾斜角可以看出它们的扰动程度。这些岩石的相—岩性特征、其中没有动物和植物,以及其他迹象表明,红色矿床的形成是在大陆条件下形成的。1-k井发现的二叠系-三叠系石油标志具有重要意义。这些石油的发现也引起了人们的兴趣,因为它们是在观测到石油的地区发现的。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
To the issue of the results of drilling a 1-k core well in Zverinogolovskoye district of Kurgan region
   This article presents the results of drilling a 1-k core well in Zverinogolovskoye district of Kurgan region and the study of core material. A number of researchers have doubts about the fact that the reason of periodic appearance of an oil film on the Alabuga River was the migration of oil from the depths. Some people assumed that it could get to the river in a small amount by accident, for example, farmers spilled it during fieldwork. In 1959, 1-k and 2-k wells were drilled in order to check and study oil occurrences along the Alabuga River. Core wells 1-k and 2-k have traversed the cover deposits of the Meso-Cenozoic and have exposed the basement rocks represented by red flowers of presumably Permian-Triassic age. This made it possible to study the lithology and stratigraphy of the sediments, which were involved in the structure of the area. The angles of inclination of red-colored rocks measured by the core of the 1-k well give an idea of the degree of their disturbance. The facies-lithological features of these rocks, the absence of fauna and flora in them, and other signs indicate that the formation of red-colored deposits occurred under continental conditions. The signs of Permian-Triassic oil found in the 1-k well are of fundamental importance. These oil occurrences are also of interest in the fact that they were detected in the area, where oil was observed to the surface.
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